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Images of Taiwan and Japan and Goddard Space Flight Center (GSFC)
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Haze Over Eastern China
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Haze Over Eastern China |
| Description |
*Haze Over Eastern China* The widespread pall of haze and pollution continued to hang over eastern China on February 15, 2004. Some of the pollution can be seen blowing over and just north of Taiwan and eastward far out to sea over the Pacific Ocean in this true-color image acquired by the Sea-viewing Wide Field-of-view Sensor (SeaWiFS). The strong winds blowing over eastern China have several other effects evident in this scene. Note the patterns of suspended sediments (light browns and turquoise) in the East China Sea, which are being churned up in the water column by the strong winds. These sediments are being washed out of the mouth of the Yangtze River and Hangzhou Bay in such abundance that they color the water a deep caramel along a long stretch of coastline, making it almost indistinguishable from land in some areas. Note also the cloud vortex streets extending southward from Korea and Japan, as well as the brownish dust and haze streaming eastward north of Tokyo. Image courtesy the SeaWiFS Project, [ http://seawifs.gsfc.nasa.gov ] NASA/Goddard Space Flight Center, and ORBIMAGE [ http://www.orbimage.com/ ] |
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Super Typhoon Halong in West
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Super Typhoon Halong in Western Pacific |
| Description |
On July 14, 2002, Super Typhoon Halong was east of Taiwan (left edge) in the western Pacific Ocean. At the time this image was taken the storm was a Category 4 hurricane, with maximum sustained winds of 115 knots (132 miles per hour), but as recently as July 12, winds were at 135 knots (155 miles per hour). Halong has moved northwards and pounded Okinawa, Japan, with heavy rain and high winds, just days after tropical Storm Chataan hit the country, creating flooding and killing several people. The storm is expected to be a continuing threat on Monday and Tuesday. This image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) on the Terra satellite on July 14, 2002. Please note that the high-resolution scene provided here is 500 meters per pixel. For a copy of the scene at the sensor's fullest resolution, visit the MODIS Rapid Response Image Gallery. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Conson (07W)
| Title |
Typhoon Conson (07W) |
| Description |
Typhoon Conson began as a weak tropical depression almost 12 days ago in the West Pacific south of the western Caroline Islands. The system moved steadily west-northwest without gaining any strength as it passed through the central Philippines. On the 2nd of June 2004, Conson emerged into the South China Sea west of the Philippines. Between the 4th and 7th, Conson traversed a slow loop over the South China Sea west of the main northern island of Luzon and strengthened into a tropical storm. On the 7th, Conson began moving towards the north-northeast and gathered enough strength to become a typhoon. The system continued its movement towards the north-northeast on the 8th bringing it closer to southern Taiwan. The system also continued to strengthen. On the 9th, Typhoon Conson passed through the Bashi Channel just south of Taiwan before passing east of the island. The Tropical Rainfall Measuring Mission (TRMM) satellite captured these images of Conson showing the storm's evolution from a tropical storm into a typhoon. The first image was taken at 17:32 UTC on 5 June 2004. It shows the horizontal distribution of rain intensity. Rain rates in the center swath are from the TRMM Precipitation Radar (PR), while rain rates in the outer swath are from the TRMM Microwave Imager (TMI). The rain rates are overlaid on infrared (IR) data from the TRMM Visible Infrared Scanner (VIRS). At the time of the first image, Conson still just a tropical storm with winds estimated at 45 knots (52 mph) by the Joint Typhoon Warning Center. TRMM shows that the storm has a well-defined circulation but lacks a complete eyewall with only moderate (green) rain intensities immediately west of the center. Isolated heavier rain (red areas) occurs in the outer rainbands. The next image taken at 16:24 UTC on the 8th shows a much stronger storm. The rainbands are tightly wrapped around the center which now contains intense (dark red areas) rain areas in the northern and eastern part of the eyewall. These intense rainrates show where heat is being released that fuels the storm. The typhoon is now over the Luzon Straight between the northern Philippines and southern Taiwan and has winds of 90 knots (104 mph). The next image was taken at the same time and shows a vertical slice through the center of the storm looking east. It shows the convection on the east side of the storm is much taller (blue areas above the yellow areas) and more intense (dark red area) than on the west side. The last set of images were taken at 16:14 UTC on the 10th as Conson was approaching the southern islands of Japan. At this time, Conson is starting to become extratropical as it accelerates to the northeast. The top down image reveals that the center has become ragged and disorganized. Some intense rainfall (dark reds) still exists north of the center and in a trailing rainband. The vertical slice taken through the convection north of the center looking east shows an area of intense rain (dark red area), and evidence of a bright band (horizontal red/yellow layer). Bright bands are brought about by melting of larger ice particles. This final image also shows that the convective towers are not as deep as they were earlier (blue areas above the yellow areas). TRMM is a joint mission between NASA and the Japanese space agency JAXA. Images produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC), NASA's Tropical Rainfall Measuring Mission. |
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Typhoon Ewiniar
| Title |
Typhoon Ewiniar |
| Description |
As of July 11, 2006, at least 30 people in China and 5 in Korea had died as a result of flooding and mudslides caused by Typhoon Ewiniar. The storm began as a tropical depression on June 30, 2006, southeast of Palau in the northern West Pacific. Ewiniar tracked generally north-northwestward before turning north to pass east of the Philippines and Taiwan. The storm made landfall in South Korea on July 10. Ewiniar was rated a Category 4 typhoon at its peak, with maximum sustained winds estimated at 240 kilometers per hour (150 miles per hour) while it was east of the Philippines on July 5. Ewiniar then slowly weakened as it passed by the coast of China before striking the Korean Peninsula as a tropical storm. Rainfall totals are shown here for the period June 29 to July 10, 2006, for the western Pacific region. The highest rainfall totals trace out Ewiniar's path, with maximum amounts around 600 millimeters or more (shown in red). These heavy amounts occurred offshore. The east-west oriented bands of moderate to isolated heavy rainfall (shown in green and red) over the east coast of China and southeast of Japan are associated with another weather system unrelated to Typhoon Ewiniar. That system brought rain to the same area during this period. The rainfall analysis above is from the Multi-satellite Precipitation Analysis, which uses data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to calibrate precipitation estimates. This product was developed by the precipitation research team in the Laboratory for Atmosphere at NASA Goddard Space Flight Center. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Typhoon Ewiniar
| Title |
Typhoon Ewiniar |
| Description |
As of July 11, 2006, at least 30 people in China and 5 in Korea had died as a result of flooding and mudslides caused by Typhoon Ewiniar. The storm began as a tropical depression on June 30, 2006, southeast of Palau in the northern West Pacific. Ewiniar tracked generally north-northwestward before turning north to pass east of the Philippines and Taiwan. The storm made landfall in South Korea on July 10. Ewiniar was rated a Category 4 typhoon at its peak, with maximum sustained winds estimated at 240 kilometers per hour (150 miles per hour) while it was east of the Philippines on July 5. Ewiniar then slowly weakened as it passed by the coast of China before striking the Korean Peninsula as a tropical storm. Rainfall totals are shown here for the period June 29 to July 10, 2006, for the western Pacific region. The highest rainfall totals trace out Ewiniar's path, with maximum amounts around 600 millimeters or more (shown in red). These heavy amounts occurred offshore. The east-west oriented bands of moderate to isolated heavy rainfall (shown in green and red) over the east coast of China and southeast of Japan are associated with another weather system unrelated to Typhoon Ewiniar. That system brought rain to the same area during this period. The rainfall analysis above is from the Multi-satellite Precipitation Analysis, which uses data from NASA's Tropical Rainfall Measuring Mission (TRMM) satellite to calibrate precipitation estimates. This product was developed by the precipitation research team in the Laboratory for Atmosphere at NASA Goddard Space Flight Center. TRMM is a joint mission between NASA and the Japanese space agency, JAXA. Image produced by Hal Pierce (SSAI/NASA GSFC) and caption by Steve Lang (SSAI/NASA GSFC). |
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Typhoon Man-Yi
| Title |
Typhoon Man-Yi |
| Description |
On July 12, 2007, Super Typhoon Man-Yi was a huge spiral of clouds, intense winds, and powerful thunderstorms as it arced northward over the western Pacific toward the southern end of the islands of Japan. Though far offshore, the Category 4 Super Typhoon [ http://www.nhc.noaa.gov/aboutsshs.shtml ] was large enough that the outer bands of storm clouds were bringing wind and rain to Taiwan. Forecasts as of July 12 were calling for the storm to weaken as it traveled through the island chain and to reach Tokyo as a milder, but still powerful, typhoon on or around July 15. The Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite acquired this photo-like image at 2:05 p.m. local time (5:05 UTC). Very near the same time MODIS was observing the storm, the Joint Typhoon Warning Center [ https://metocph.nmci.navy.mil/jtwc.php ] estimated Man-Yi's sustained winds to be over 240 kilometers per hour (145 miles per hour). The satellite image confirms that Man-Yi was a powerful Super Typhoon. The storm has the hallmark tightly wound arms that spiral around a well-defined, circular eye. The symmetrical spirals, clear eye, and intense storm clouds around the eyewall (innermost band of clouds) are all features regularly seen in satellite images of other particularly powerful typhoons. The high-resolution image provided above is at MODIS' full spatial resolution (level of detail) of 250 meters per pixel. The MODIS Rapid Response System provides this image at additional resolutions. [ http://rapidfire.sci.gsfc.nasa.gov/gallery/?2007193-0712/Man-Yi.A2007193.0505 ] You can download a 250-meter-resolution Super Typhoon Man-Yi KMZ file [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jul2007/Man-Yi.A2007193.0505.250m.kmz ] for use with Google Earth. [ http://earth.google.com/download-earth.html ] NASA image by Jeff Schmaltz, MODIS Rapid Response Team, [ http://rapidfire.sci.gsfc.nasa.gov ] Goddard Space Flight Center. |
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Typhoon Nock-Ten strikes Tai
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| Title |
Typhoon Nock-Ten strikes Taiwan |
| Description |
Typhoon Nock-Ten hammered Taiwan with heavy rains and strong winds on October 25, 2004, killing at least four, according to media reports. Heavy rains drenched northeastern Taiwan, triggering extensive flooding. Though winds had dropped to about 170 kilometers per hour (100 mph) when the storm blew ashore, at its height, Nock-Ten?s maximum sustained winds reached 204 kilometers per hour (127 mph) with stronger gusts. This image of the storm was acquired on October 24, by the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA?s Terra [ http://terra.nasa.gov/ ] satellite a few hours after the storm began to weaken. Nock-Ten, ?bird? in Laotian, is the sixth typhoon to strike Taiwan and the 24th to develop in the western Pacific this year. After moving across northern Taiwan, the storm curved east over the East China Sea and weakened into an extra-tropical depression as it approached Japan?s southern islands on October 26. NASA image created by Jesse Allen, Earth Observatory, using data obtained from the MODIS Rapid Response team. |
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Typhoon Shanshan
| Title |
Typhoon Shanshan |
| Description |
Typhoon Shanshan formed on September 10, 2006, in the western Pacific off the coast of the Philippine Islands. Over the course of the next 36 hours, it grew from a tropical depression (area of low air pressure) to a typhoon, reaching Category 4 [ http://www.nhc.noaa.gov/aboutsshs.shtml ] strength as it passed Taiwan on September 15. Typhoon Shanshan stayed at Category 4 (a Super Typhoon) for two days, starting to subside only late in the day on September 16. As of September 19, the typhoon was projected to pass on a northeasterly track through the straits between the Korean Peninsula and southern Japan, and to curve east to cross Hokkaido. This photo-like image was acquired by the Moderate Resolution Imaging Spectroradiometer (MODIS) [ http://modis.gsfc.nasa.gov/ ] on the Aqua [ http://aqua.nasa.gov/ ] satellite on September 18, 2006, at 1:25 p.m. local time (04:25 UTC). Shanshan at the time of this image had a well-defined spiral shape, with a distinct but cloud-filled ("closed") eye. Shanshan had sustained winds of around 140 kilometers per hour (85 miles per hour) at the time this satellite image was acquired, according to the University of Hawaii's Tropical Storm Information Center. [ http://www.solar.ifa.hawaii.edu/Tropical/tropical.html ] Though no longer a super typhoon by this time, Agence France Presse reported nine deaths in southern Japan attributed to the storm, as well at least 310 injuries, and one person missing. Risks for landslides, flooding, and strong storm surge along the western coast were expected to remain high as the storm traveled near the western coastline. NASA image created by Jesse Allen, Earth Observatory, using data provided courtesy of the MODIS Rapid Response [ http://rapidfire.sci.gsfc.nasa.gov/ ] team. |
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Typhoon Sinlaku
| Title |
Typhoon Sinlaku |
| Description |
On September 4, 2002, Typhoon Sinlaku passed directly above the Japan?s Okinawan island chain, generating winds of 145 kph (90 mph) and torrential rains. The typhoon knocked out electricity to tens of thousands of homes, injured 25 residents, and possibly killed five Filipino sailors. Currently, the typhoon is making its way toward Taiwan, packing sustained winds of 104 miles (167 kilometers) per hour. Taiwanese residents are shoring up their houses with sand bags and pulling their boats out of the water. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC. |
|
Typhoon Sinlaku
| Title |
Typhoon Sinlaku |
| Description |
On September 4, 2002, Typhoon Sinlaku passed directly above the Japan?s Okinawan island chain, generating winds of 145 kph (90 mph) and torrential rains. The typhoon knocked out electricity to tens of thousands of homes, injured 25 residents, and possibly killed five Filipino sailors. Currently, the typhoon is making its way toward Taiwan, packing sustained winds of 104 miles (167 kilometers) per hour. Taiwanese residents are shoring up their houses with sand bags and pulling their boats out of the water. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC. |
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Typhoon Soudelor
| Title |
Typhoon Soudelor |
| Description |
On Tuesday, June 17, 2003 the MODIS instrument onboard the Aqua spacecraft captured this true-color image of Tropical Cyclone Soudelor in the Philippine Sea. Soudelor (07W) is centered near 22.0 degrees north and 123.5 degrees east with sustained winds near 105 mph and gusts to 125 mph. The typhoon is moving to the north-northeast at 12 mph and this track is expected to continue over the next 24-36 hours, so Soudelor will pass to the west of the Ryukyu Islands and move near Kyushu. Rain and thunderstorms will cause locally heavy rainfall from Taiwan through the Ryukyu Islands and into southern Japan. Image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team at NASA GSFC. |
|
Typhoon Soudelor
| Title |
Typhoon Soudelor |
| Description |
*animations:* small movie (972 KB MPEG)large movie [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2003/soudelor.qt ] (2.5 MB QuickTime) After traversing through the western Pacific over the past week, Tropical Cyclone Soudelor (07W) was beginning the end of its life cycle as it passed through the Korean Strait. Soudelor was named a Tropical Storm just west of the central Philippines at 12:00 UTC on the June 13, 2003. In the days following, the storm slowly skirted east of the Philippines where it delivered several inches of rain to the central islands as seen in the TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) from the NASA Goddard Space Flight Center. Once past the Philippines, Soudelor took a more northerly track staying well east of the island of Taiwan and was elevated to typhoon status at 18:00 UTC on the June 16. After briefly reaching a strength of category 4 on the June 18, Soudelor began to weaken as it left the East China Sea and passed through the Korean Strait into the Sea of Japan. TRMM was able to capture Soudelor's the swath of heavy rainfall extending from east of the Philippines all the way into southern Japan where the cyclone interacted with a frontal system. This rainmap shows the total rainfall accumulation for the period June 13-20, 2003. The heaviest rainfall totals were found just off the southern coast of Korea and were a result of Soudelor's interaction with the frontal system. Although parts of southern Japan are shown to have received several inches of rain, fortunately the heaviest amounts remained offshore. NASA's TRMM or Tropical Rainfall Measurement Mission features a spaceborne weather radar built by the Japanese space agency NASDA. In operation for five years, TRMM has provided unprecedented views of tropical rain events around the globe. For more information on TRMM, please visit the TRMM website. Image and movie courtesy of Hal Pierce, TRMM Project, NASA Goddard Space Flight Center. |
|
Typhoon Soudelor
| Title |
Typhoon Soudelor |
| Description |
*animations:* small movie (972 KB MPEG)large movie [ http://earthobservatory.nasa.gov/NaturalHazards/Archive/Jun2003/soudelor.qt ] (2.5 MB QuickTime) After traversing through the western Pacific over the past week, Tropical Cyclone Soudelor (07W) was beginning the end of its life cycle as it passed through the Korean Strait. Soudelor was named a Tropical Storm just west of the central Philippines at 12:00 UTC on the June 13, 2003. In the days following, the storm slowly skirted east of the Philippines where it delivered several inches of rain to the central islands as seen in the TRMM-based, near-real time Multi-satellite Precipitation Analysis (MPA) from the NASA Goddard Space Flight Center. Once past the Philippines, Soudelor took a more northerly track staying well east of the island of Taiwan and was elevated to typhoon status at 18:00 UTC on the June 16. After briefly reaching a strength of category 4 on the June 18, Soudelor began to weaken as it left the East China Sea and passed through the Korean Strait into the Sea of Japan. TRMM was able to capture Soudelor's the swath of heavy rainfall extending from east of the Philippines all the way into southern Japan where the cyclone interacted with a frontal system. This rainmap shows the total rainfall accumulation for the period June 13-20, 2003. The heaviest rainfall totals were found just off the southern coast of Korea and were a result of Soudelor's interaction with the frontal system. Although parts of southern Japan are shown to have received several inches of rain, fortunately the heaviest amounts remained offshore. NASA's TRMM or Tropical Rainfall Measurement Mission features a spaceborne weather radar built by the Japanese space agency NASDA. In operation for five years, TRMM has provided unprecedented views of tropical rain events around the globe. For more information on TRMM, please visit the TRMM website. Image and movie courtesy of Hal Pierce, TRMM Project, NASA Goddard Space Flight Center. |
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Typhoon Talim
| Title |
Typhoon Talim |
| Description |
Typhoon Talim was a building storm in the western Pacific several hundred kilometers south of Japan when the Moderate Resolution Imaging Spectroradiometer (MODIS [ http://modis.gsfc.nasa.gov ]) on NASA's Aqua [ http://aqua.nasa.gov/ ] satellite captured this image on August 29, 2005. At this time, 1:25 p.m. Tokyo time, it had sustained winds of around 180 kilometers an hour (115 miles per hour) and was heading towards Taiwan at around 15 miles per hour. As of August 30, was being predicted to continue to gather up stronger winds and to strike Taiwan on September 2, and then continue across the Taiwan Strait to make landfall again on mainland China perhaps a day later. The typhoon should reach Category 4 strength, making it another super typhoon, by the time it strikes Taiwan, but should be a weaker Category 1 regular typhoon when it comes ashore on the mainland. The large image provided above has a spatial resolution of 500 meters per pixel. The MODIS Rapid Response Team provides the image in additional resolutions [ http://rapidfire.sci.gsfc.nasa.gov/gallery/?2005241-0829/Talim.A2005241.0425 ], including MODIS' maximum resolution of 250 meters per pixel. NASA image courtesy Jeff Schmaltz, MODIS Land Rapid Response Team [ http://rapidfire.sci.gsfc.nasa.gov ] at NASA GSFC |
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Typhoon Man-Yi: Natural Haza
…
nasa, nasanaturalhazards
On July 12, 2007, Super Typh
…
manyi_amo_2007193
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2007-07-12 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
manyi_amo_2007193 |
|
Typhoon Ewiniar: Natural Haz
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
ewiniar_mpa_2006191
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2006-07-10 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
ewiniar_mpa_2006191 |
|
Typhoon Sinlaku: Natural Haz
…
nasa, nasanaturalhazards
Typhoon Sinlaku can be seen
…
sinlaku_terra_02sep02
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2002-09-02 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
sinlaku_terra_02sep02 |
|
Typhoon Conson (07W): Natura
…
nasa, nasanaturalhazards
* eoimages.gsfc.nasa.gov/ima
…
trmm_conson_5june1732
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2004-06-05 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
trmm_conson_5june1732 |
|
Typhoon Soudelor: Natural Ha
…
nasa, nasanaturalhazards
animations: /NaturalHazards/
…
soudelor_trm2003170
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2003-06-19 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
soudelor_trm2003170 |
|
Typhoon Sinlaku: Natural Haz
…
nasa, nasanaturalhazards
Typhoon Sinlaku can be seen
…
sinlaku.AMO2002246
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2002-09-03 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
sinlaku.AMO2002246 |
|
Typhoon Sinlaku: Natural Haz
…
nasa, nasanaturalhazards
Typhoon Sinlaku can be seen
…
sinlaku.AMO2002246
| mediatype |
IMAGE |
| mediatype |
image |
| date |
2002-09-03 |
| creator |
NASA -- NASA Image Of The Day |
| identifier |
sinlaku.AMO2002246 |
|
|
